2003 Seattle Annual Meeting (November 2–5, 2003)
Paper No. 13-9
Presentation Time: 10:25 AM-10:40 AM

CONDUIT FLOW: PATHWAYS TO POOR ASR RECOVERY AND SURFACEWATER CONTAMINATION IN FLORIDA

BACCHUS, Sydney T., Applied Environmental Svcs, P. O. Box 174, Athens, GA 30603, appliedenvirserv@mindspring.com, KINCAID, Todd R., Hazlett-Kincaid, Inc, 505 Arlington, Suite 203, Reno, NV 89509, kincaid@hazlett-kincaid.com, and HAZLETT, Timothy J., Hazlett-Kincaid, Inc, 2012-A North Point Blvd, Tallahassee, FL 32308

Construction of 330 ‘aquifer storage and recovery’ (‘ASR’) wells is a key component of the approximately $8 billion Congressional appropriation for south Florida’s Everglades Restoration Plan (ERP). Injected ‘recharge’ fluids can include untreated stormwater runoff containing toxic agricultural and urban contaminants, as well as treated effluent. Similar wells in Florida (20 to hundreds of meters deep) are used for aquifer-injection of minimally-treated sewage effluent, stormwater runoff, and agricultural wastewater. Sewage effluent is injected into the aquifer via approximately 1,000 shallow wells throughout the Florida Keys.

‘Recovery’ efficiency (at 250 mg/L chloride concentration) reported by USGS was 3.1%, 2.7%, and 7.2% (‘storage’ periods: 0, 8, and 5 days, respectively) for Lake Okeechobee ‘ASR’ wells proposed for use in the northern vicinity of the ERP. Actual ‘recovery’ efficiency was lower, since chloride concentrations of injected ‘recovery’ fluids were 150, 100, and 70 mg/L, respectively, for those tests. Dye tracer tests conducted this year by USGS in the Biscayne (surficial) aquifer, south of Lake Okeechobee, revealed groundwater travel times of several hours over distances predicted to require days. Evidence that injected fluids resurface in nearshore waters (induced discharge) is seen in stable nitrogen isotope data from macroalgae smothering reefs in southeast Florida.

Those results reflect conduit flow of injected fluids that can cause large-scale subsurface discharge of nutrients and other contaminants into Florida’s sensitive surface waters, including the surf zone. Poor ‘recovery’, rapid travel times, and discharge points for the karst aquifer system are not addressed by groundwater models used for decision-making. Similar flow responses have been addressed in other areas of the regional Floridan aquifer system using a finite-element groundwater model. This approach can identify probable discrete flow paths and discharge points.

2003 Seattle Annual Meeting (November 2–5, 2003)
Session No. 13
Flow and Biogeochemical Processes at the Interface Between Surface Water and Groundwater
Washington State Convention and Trade Center: 608
8:00 AM-12:00 PM, Sunday, November 2, 2003

Geological Society of America Abstracts with Programs, Vol. 35, No. 6, September 2003, p. 50

© Copyright 2003 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.